(Table 4) Isotopic compositions of samples from ODP Hole 107-650A, Sediment type
| Cobertura |
LATITUDE: 39.356700 * LONGITUDE: 13.900800 * DATE/TIME START: 1986-01-02T22:38:00 * DATE/TIME END: 1986-01-09T14:30:00 * MINIMUM DEPTH, sediment/rock: 596.89 m * MAXIMUM DEPTH, sediment/rock: 601.94 m |
|---|---|
| Data(s) |
14/01/2007
|
| Formato |
text/tab-separated-values, 63 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.711225 doi:10.1594/PANGAEA.711225 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.711309 Dekov, Vesselin M; Kamenov, George D; Savelli, Carlo; Stummeyer, Jens; Marchig, Vesna (2007): Origin of basal dolomitic claystone in the Marsili Basin, Tyrrhenian Sea. Marine Geology, 236(3-4), 121-141, doi:10.1016/j.margeo.2006.10.021 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #107-650A; Chromatographic; delta 13C; delta 18O; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Joides Resolution; Lead 206/Lead 204 ratio; Lead 207/Lead 204 ratio; Lead 208/Lead 204 ratio; Leg107; Mass spectrometer Finnigan MAT 252; Mass spectrometer Micromass Sector 54; Ocean Drilling Program; ODP; ODP sample designation; Sample code/label; Strontium 87/Strontium 86 ratio; Tirreno Sea |
| Tipo |
Dataset |
